A geochemical perspective on Parisian urban history based on U–Th dating, laminae counting and yttrium and REE concentrations of recent carbonates in underground aqueducts

Edwige Pons-Branchu (1, 2) , Eric Douville (1, 2) , Matthieu Roy-Barman (1, 3) , Emmanuel Dumont (4) , Philippe Branchu (5) , François Thil (1, 2) , Norbert Frank (1, 2) , Louise Bordier (1, 3) , Wolfgang Borst (6)

1 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
2 GEOTRAC - Géochrononologie Traceurs Archéométrie
3 GEDI - Géochimie Des Impacts
4 CESAER - Centre d'Economie et de Sociologie Rurales Appliquées à l'Agriculture et aux Espaces Ruraux
5 TEAM - Transferts et interactions liés à l'eau en milieu construit
6 Cerema - Centre d'Etudes et d'Expertise sur les Risques, l'Environnement, la Mobilité et l'Aménagement

Two laminated carbonate deposits from the wall of an underground aqueduct, built between the 13 th and 15 th century, in Paris, France, were studied to provide historical information about nearby human occupation and urban development. To obtain a robust chronology for these small (29 and 45 mm thickness) and very young deposits< 800 a based on the probable date of aqueduct construction, we adopted two methods: laminae counting and U-Th analysis. For laminae, we tested the hypothesis that their deposition is biannual. Concerning U-Th dating, the influence of inherited 230 Th on calculated ages is discussed and detrital 230 Th/ 232 Th values for each speleothem was determined using stratigraphic constraints and found to be significantly different despite their close proximity. In these speleothems, that precipitated over approximately 300 a according to U-Th dating, the number of laminae is similar, and two laminae were deposited each year. A lamina-counting chronology was used to interpret the rare earth elements and yttrium content (REE + Y) variations measured by ICP-QMS as historical variations in water quality in relation with the anthropogenic use of these elements, with a marked increase in the REE + Y concentrations since the second half of the twentieth century. A marked negative Ce anomaly in the NASC-normalized REE trend is evidenced, and is more pronounced for post 1850s. This anomaly could be due to prior precipitation of Ce 4+ before the water reached the aqueduct, related to a high organic matter content of the water in oxidizing conditions. The increase in the Ce anomaly could indicate a second source of water, from a wastewater collection system or a modern water conveyance system. We thus demonstrate the interest of using these annual carbonate deposits in urban areas as a proxy for the history of urbanization or human activities. Keywords : urban speleothems, relative chronology, U-Th dating, urbanization impact on water quality, Rare Earth Elements, Yttrium. Highlights:  We test the potential of urban speleothems as a natural archive for the history of the impact of urbanization on water chemistry  We compare absolute (U-Th) and relative chronologies for young speleothems  We discuss corrections for detrital 230 Th for U-Th dating using stratigraphic constraints  We evidence a high REE and yttrium content in infiltration waters in Paris since the mid-twentieth century  We discuss the presence of a negative Ce anomaly in the urban speleothems

Mots clés: Relative chronology; Urban speleothems; Yttrium; Urbanization impact on water quality; Rare earth elements; U–Th dating

Domaines: Sciences de l'environnement; Géochimie

Edwige Pons-Branchu, Eric Douville, Matthieu Roy-Barman, Emmanuel Dumont, Philippe Branchu, et al.. A geochemical perspective on Parisian urban history based on U–Th dating, laminae counting and yttrium and REE concentrations of recent carbonates in underground aqueducts. Quaternary Geochronology, 2014, 24, pp.44-53. ⟨10.1016/j.quageo.2014.08.001⟩. ⟨hal-02428406⟩